When we approach foot of beach and we face us to the immensity of the sea to every fisherman, experienced or new, always arises him the great doubt, ¿and now, where I place me?

Reading the beach, pending subject.

The reading of the coast is task of a lot of dedication and this always based on the own experience. The fact to determine in an immense sand which is the place but appropriate to carry out the better captures according to the state of tides, winds and currents is not without doubt easy task.

Nevertheless the observer that know to read those small appreciations that the sea gives us, will have to its favor the indications that showed where and as to be placed al to arrive at the positions of fishing with greater efficacy and percentage of success.

In our Atlantic water, affected by hardly tides that can change literally a zone in the interval of six hours, the to locate an appropriate position can despair al but calm. So if you are willing to accompany me for a walk by the beach we will try to discover together some of those small trails that will serve to orient us.

The depth.

The fact to locate a deep zone al reach of our canes is without doubt a good trick. These depressions permit the I travel continuous of predatory species that seek actively the fish of smaller size that are found concentrated on these zones being fed of the fauna and flora that remain collected in the pots.

One of the better ways than I know to be able to locate them is for the reading of the waves; in the Atlantic zone the successions of waves a cadence determined for three waves is produces by that arrive from forms successive, are the acquaintances by the nickname of "the three marías", this cadence in the oceanic waves that arrive at ours coastal they will be seen slowed down in proportion to the depth of the zone Coastal, being able to be read of an in a with greater interval in these zones.

To broadly speaking the interaction of the depth of the coastal zone we can reflect it in the following graphics and that without doubt helped us to understand the process.

As we see the depth of the coastal zone acted in decremento of the velocity of the waves, with which we can decree that to a zone of greater cadence a zone of greater depth corresponds.